In some articles, the oxygen cage surrounding the rare-earth ion in orthoferrites like La3+ in LaFeO3 is described as dodecahedral, whereas in others, it is described as cuboctahedral. Which definition is more precise? then why?

Based on orthoferrites' distorted structure, the first nearest Oxygen ions to La3+ are 8 O2- ions, and the second nearest are 4 O2- ions. Can we, therefore, refer to the oxygen skeleton surrounding La3+ as a hexahedron while neglecting the second neighbors?

Because the Gd3+ ion in GdFeO3 is defined as an 8-coordinated ion.

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